Dinoflagellate
The
dinoflagellates are a large group of
flagellate protists. Most are marine
plankton, but they are common in
fresh water habitats as well. About half of all dinoflagellates are
photosynthetic, and these make up the largest group of
algae aside from the
diatoms. Some species, called
zooxanthellae, are endosymbionts of marine animals and protozoa, and play an important part in the biology of
coral reefs. Other dinoflagellates are colorless predators on other protozoa, and a few forms are
parasitic.
Most dinoflagellates are unicellular forms with two dissimilar flagella. One of these extends towards the posterior, called the
longitudinal flagellum, while the other forms a lateral circle, called the
transverse flagellum. In many forms these are set into grooves, called the
sulcus and
cingulum. The transverse flagellum provides most of the force propelling the cell, and often imparts to it a distinctive whirling motion, which is what gives the name dinoflagellate refers to (Greek
dinos, whirling).
Dinoflagellates have a complex cell covering called an
amphiesma, composed of flattened
vesicles, called
alveoli. In some forms, these support overlapping
cellulose plates that make up a sort of armor called the
theca. These come in various shapes and arrangements, depending on the species and sometimes stage of the dinoflagellate. Fibrous extrusomes are also found in many forms. Together with various other structural and genetic details, this organization indicates a close relationship between the dinoflagellates,
Apicomplexa, and
ciliates, collectively referred to as the
alveolates.
The
chloroplasts in most photosynthetic dinoflagellates are bound by three membranes, suggesting they were probably derived from some ingested alga, and contain chlorophylls
a and
c and fucoxanthin, as well as various other accessory
pigments. However, a few have chloroplasts with different pigmentation and structure, some of which retain a
nucleus. This suggests that chloroplasts were incorporated by several endosymbiotic events involving already colored or secondarily colorless forms. The discovery of plastids in Apicomplexa have led some to suggest they were inherited from an ancestor common to the two groups, but none of the more basal lines have them.
Dinoflagellates have a peculiar form of
nucleus, called a
dinokaryon, in which the
chromosomes are attached to the nuclear membrane. These lack
histones and remained condensed throughout interphase rather than just during
mitosis, which is closed and involves a unique external spindle. This sort of nucleus was once considered to be an intermediate between the nucleoid region of
prokaryotes and the true nuclei of
eukaryotes, and so were termed
mesokaryotic, but now are considered advanced rather than primitive traits. In most dinoflagellates, the nucleus is dinokaryotic throughout the entire life cycle.
Most dinoflagellates are
haploid, and reproduce primarily through
fission, but sexual reproduction also occurs. This takes place by fusion of two individuals to form a
zygote, which may remain mobile in typical dinoflagellate fashion or may form a resting cyst, which later undergoes
meiosis to produce new haploid cells. Dinoflagellate cysts are found as common microfossils from the
Triassic period onwards. A few are known from as far back as the
Silurian, and it is likely that some of the older
acritarchs also represent dinoflagellates.
Dinoflagellates sometimes
bloom in concentrations of more than a million cells per mililitre. Some species produce neurotoxins, which in such quantities kill fish and accumulate in filter feeders such as
shellfish, which in turn may pass them on to people who eat them. This phenomenon is called a
red tide, from the color the bloom imparts to the water. Some colorless dinoflagellates may also form toxic blooms, such as
Pfiesteria. It should be noted that not all dinoflagellate blooms are dangerous. Bluish flickers visible in ocean water at night often come from blooms of
bioluminescent dinoflagellates, which emit short flashes of light when disturbed.
The dinoflagellates were first defined by
Otto Bütschli in 1885 as the flagellate order Dinoflagellida. Botanists treated them as a division of algae, named Pyrrhophyta after the bioluminscent forms (Greek
pyrrhos, fire). They have also been called the Dinophyta or Dinoflagellata. At various times the
cryptomonads, ebriids, and ellobiopsids have been included here, but do not appear closely related.